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Pliocene-Pleistocene lacustrine system in the Eastern Cordillera Basin, Colombia: Paleoenvironmental implications for diatomite deposition
被引:1
|作者:
Gomez-Neita, Juan Sebastian
[1
,2
,3
]
Rocio Manosalva-Sanchez, Sandra
[2
]
Evangelista Nogueira, Anna Andressa
[3
]
Enario Naranjo-Merchan, Wilson
[2
]
Rodrigues Nogueira, Afonso Cesar
[3
]
机构:
[1] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Ave Bento Goncalves 9500, Porto Alegre, RS, Brazil
[2] Univ Pedag & Tecnol Colombia, Grp Invest Ingn Geol, Escuela Ingn Geol, Fac Secc Sogamoso, Calle 4 Sur 15-134, Sogamoso, Boyaca, Colombia
[3] Univ Fed Para, Inst Geociencias, Programa Posgrad Geol & Geoquim, Ave Augusto Correa 01, BR-66075110 Belem, Para, Brazil
关键词:
Diatoms;
Lacustrine;
Facies;
Quaternary;
Tilata Formation;
Aulacoseira;
PALYNOLOGICAL RECORD;
BENTHIC DIATOMS;
ORGANIC-MATTER;
POLLEN RECORDS;
NORTHERN ANDES;
CLIMATE-CHANGE;
LAKE;
RIVERS;
ASSEMBLAGES;
QUATERNARY;
D O I:
10.1016/j.sedgeo.2022.106274
中图分类号:
P5 [地质学];
学科分类号:
0709 ;
081803 ;
摘要:
The Plio-Pleistocene Tilata Formation records a tectonic paleo-lake system in the Colombian Andes. This unit exhibits recurrent episodes of volcanism and diatomite deposits. Outcrop-based facies analysis of eight stratigraphic sections varying in thickness from 4 to 40 m indicates variations in the sediment supply, accommodation space, climatic conditions, water depth, and organic activity. Fourteen sedimentary facies are grouped into three facies associations (FAs) representative of alluvial, fluvial, and lacustrine settings. FA1 (alluvial fan deposits) corresponds to conglomerates, sandstones, and subordinated mudstones. FA2 (mixed fluvial system) represents sandy conglomerates, cross-bedded/massive sandstones, organic-rich mudstones, lignites, and diatomaceous mudstones. FA3 (lacustrine) comprises mainly organic-rich mudstones, diatomites, laminated sandstones, and tephra layers. The Upper Tilata Formation reflects the evolution of an overfilled to a balanced-fill lake with a progradational-retrogrational-progradational stacking pattern. The organic facies revealed variations in the origin of the Amorphous Organic Matter (AOM) from aquatic to terrestrial, indicating episodes of shallowing when terrestrial conditions dominated. Seven families, eight genera, and eleven diatom species were identified in diatomites and diatomaceous mudstones, mainly in the lacustrine facies. The most abundant species was Aulacoseira ambigua, suggesting moderate energy in the water column (turbulence), solar light availability for photosynthesis, and mesotrophic to eutrophic conditions. The sedimentological record implies that bedrock, fluvial, pluvial, and volcanic input played a decisive role in nutrient supply for the proliferation of diatoms in the paleo-lake. This scenario is concordant with similar Quaternary depositional systems in northern South America. (c) 2022 Elsevier B.V. All rights reserved.
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